Three-dimensional mapping of salt stores in the Murra-Darling Basin, Australia - 2. Calculating landscape salt loads from airborne electromagnetic and laboratory data

被引:11
作者
Mullen, I. C.
Wilkinson, K. E.
Cresswell, R. G.
Kellett, J.
机构
[1] Bur Rural Sci, Canberra, ACT 2601, Australia
[2] Queensland Dept Nat Resources & Mines, Indooroopilly, Qld 4068, Australia
[3] CRC LEME CSIRO Land & Water, Indooroopilly, Qld 4068, Australia
来源
INTERNATIONAL JOURNAL OF APPLIED EARTH OBSERVATION AND GEOINFORMATION | 2007年 / 9卷 / 02期
关键词
airborne electromagnetic survey; salinity; salt load; pore fluids; three-dimensional mapping;
D O I
10.1016/j.jag.2006.08.005
中图分类号
TP7 [遥感技术];
学科分类号
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要
Salt is widespread in the Australian landscape - in soil, regolith and groundwater - leading to concerns that land management practices may be putting much agricultural land and important water resources at risk of salinisation. Defining the location and nature of salt stores is an important first step in understanding the processes leading to salinity of soils, streams and groundwater resources, and predicting areas that may be at risk. Airborne geophysics can define subsurface salt stores and mobilisation pathways. Airborne electromagnetics (AEM) can map the three-dimensional conductivity structure of the landscape but does not, intrinsically, quantify the amount of salt. Salinity, moisture content, porosity and mineralogy all contribute to the electromagnetic signal, and each can vary significantly throughout the landscape. In the Lower Balonne catchment, Queensland, the relationship between AEM and the amount of salt in the landscape was quantified using laboratory analyses of pore fluids from core samples. A general statistical relationship was established between AEM conductivity and salt load (defined as the product of pore fluid salinity, porosity and moisture content)-with a significant positive correlation although data were generally widely dispersed. Comparison of calculated salt load with borehole electromagnetic logs gives insight into the factors contributing to dispersion in the AEM data. The relationship transforms bulk conductivity to salt load in 5 m layers, allowing the generation of a three-dimensional map of the salt load. This is a powerful tool for identifying areas that may require monitoring and management interventions to reduce salinity risk. An example is given of salt loads beneath an established irrigation area in the Lower Balonne catchment, Queensland. Crown Copyright (c) 2006 Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:103 / 115
页数:13
相关论文
共 33 条
[1]  
[Anonymous], 163 CRC LEME
[2]  
BRAATEN R, 2003, STEPS SOLVING SALINI
[3]  
CHAMBERLAIN T, 2004, QNRM04255 QUEENSL DE
[4]  
COPPA I, 1998, EXPLOR GEOPHYS, V29, P230
[5]   Three-dimensional mapping of salt stores in the southeast Murray-Darling Basin, Australia. 1. Steps in calibration of airborne electromagnetic surveys [J].
Cresswell, RG ;
Dent, DL ;
Jones, GL ;
Galloway, DS .
SOIL USE AND MANAGEMENT, 2004, 20 (02) :133-143
[6]  
DAWES WR, 2000, 500 CISRO
[7]  
DENT D, 2002, VICTORIA UNDERCOVER, P223
[8]  
DENT D, 2003, 5 STEPS TACKLING SAL
[9]  
Dent D., 1999, LAND GENT, V3, P179
[10]  
ENGLISH P, 2004, 1804 CSIRO